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Origin and evolution of silicic magmatism at Yellowstone based on ion microprobe analysis of isotopically zoned zircons

Bindeman, Ilya N; Fu, Bin; Kita, Noriko T; Valley, John


The origin of large-volume Yellowstone ignimbrites and smaller-volume intra-caldera lavas requires shallow remelting of enormous volumes of variably 18O-depleted volcanic and sub-volcanic rocks altered by hydrothermal activity. Zircons provide probes of t

CollectionsANU Research Publications
Date published: 2008
Type: Journal article
Source: Journal of Petrology
DOI: 10.1093/petrology/egm075


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